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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Caribbean region
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Antilles
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Aymamon Limestone
Strontium Isotope Stratigraphy for Oligocene-Miocene Carbonate Systems in Puerto Rico and the Dominican Republic: Implications for Caribbean Processes Affecting Depositional History
Paleoenvironments of Quebradillas Limestone (Tertiary), Northern Puerto Rico, and Their Geologic Significance: GEOLOGIC NOTE
—White limestone with Amphistegina angulata and encrusting coralline algae;...
Stratigraphy and Petroleum Possibilities of Middle Tertiary Rocks in Puerto Rico: REPLY
Stratigraphy and Petroleum Possibilities of Middle Tertiary Rocks in Puerto Rico
Stratigraphy and Petroleum Possibilities of Middle Tertiary Rocks in Puerto Rico: DISCUSSION
Stratigraphy and Petroleum Possibilities of Middle Tertiary Rocks in Puerto Rico: DISCUSSION
V S 30 and Spectral Response from Collocated Shallow, Active‐, and Passive‐Source V S Data at 27 Sites in Puerto Rico
Effects of sea level and upwelling on development of a Miocene shallow-water tropical carbonate ramp system, Ponce, Puerto Rico
Abstract Over 72 exploration wells have been drilled on the Caribbean islands of Hispaniola and Puerto Rico over the past century, but with no commercial success. A question is whether these Caribbean oceanic islands have experienced sufficient subsidence and burial for any potential source rocks to reach maturity and produce commercial hydrocarbons. Subsurface data from previous studies were compiled into a regional depth to basement and sediment thickness map for Hispaniola, Puerto Rico and their offshore areas. The thickest basins include the Enriquillo/Cul-de-Sac basin (6.3 km), San Juan/Plateau Central basin (5 km), Azua basin (2.8 km), Cibao basin (5 km), North Coast basin (2.5 km), South Coast basin (1.3 km), Haiti sub-basin (3.7 km), Hispaniola basin (3.5 km) and San Pedro basin (3 km). One-dimensional modelling for six onland basins shows that only the Azua basin of the south-central Dominican Republic has reached sufficient maturity to place potential source rocks into the oil window. Our study shows that commercial hydrocarbons are possible in the deeper basins – Azua basin, San Juan–Plateau Central basin and Cibao basin of Hispaniola – but unlikely in the shallower basins that lack sufficient overburden for organic maturity.